Please use this identifier to cite or link to this item: http://117.252.14.250:8080/jspui/handle/123456789/8063
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dc.contributor.authorKrishan, Gopal-
dc.contributor.authorSakthivel, V.-
dc.contributor.authorRao, M.S.-
dc.contributor.authorKhobragade, S.D.-
dc.date.accessioned2026-11-11T07:18:26Z-
dc.date.available2026-11-11T07:18:26Z-
dc.date.issued2026-
dc.identifier.citationJournal of Radioanalytical and nuclear chemistryen_US
dc.identifier.urihttp://117.252.14.250:8080/jspui/handle/123456789/8063-
dc.description.abstractGroundwater radon (222Rn) poses radiological risks in Himalayan regions dominated by fractured crystalline aquifers. This study evaluates radon variability in groundwater from Tehri Garhwal (Lesser Himalayas) and compares it with previously published groundwater data from 27 sites (post-monsoon 2022) in the Siwalik foothills (Dehradun) and Gangetic alluvial plains (Haridwar). In the present study, ten groundwater samples from Tehri Garhwal were analyzed for radon, while hydro chemical and stable isotope (δ18O and δD) analyses were conducted on 13 water samples, including the ten analyzed for radon. Radon concentrations ranged from 2 to 43 Bq L⁻1, with 70% exceeding the recommended drinking-water guideline .en_US
dc.language.isoenen_US
dc.publisherSpringeren_US
dc.subjectRadonen_US
dc.subjectLesser Himalayasen_US
dc.subjectPublic health implicationsen_US
dc.subjectPost-monsoonen_US
dc.subjectHydrogeochemistryen_US
dc.subjectGroundwater recharge sourcesen_US
dc.titleRadon variability in groundwater from the lesser Himalayas to the gangetic alluvial plain, with hydrogeochemical and isotopic insights from Tehri Garhwalen_US
dc.typeArticleen_US
Appears in Collections:Research papers in International Journals



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